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<br />0017 <br /> <br /> Table 1. -Range of field measurements at all stations <br /> Dissolved <br />Sampling Number of Temperature oxygen Conductivitv pH Eh Flow <br />station measurements .C mg/L J-tS/cm mV mJ/s <br />EF - 1 19 0-10.1 8.05-10.10 78-201 7.55- 8.40 300-620 0.19-10.58 <br />Leadville 19 69- 7.5 4.39- 8.65 790-1070 6.50.7.52 265-445 .02- .15 <br />Drain <br />EF - 2 19 .1-13.1 7.30-10.90 78-460 7.65-8.67 340-608 .24-10.68 <br />AR - 1 15 .1-13.8 7.30- 9.65 60-425 7.40- 8.62 282-598 .37-20.57 <br />AR - 2 19 .1-12.9 7.25-10.90 79-350 7.45- 8.50 285-465 .37-20.57 <br />California 19 .1-18.2 5.20-11.10 600-1520 3.30-8.60 170-685 .07- .41 <br />Gulch <br />AR - 3 19 .1-13.2 7.50-10.20 80-440 7.50-9.20 150-458 .44-20.98 <br />AR - 4 15 .4-18.1 7.75-10.60 71-200 7.15-8.12 325-520 2.63-41.32 <br />AR - 5 19 .7-18.5 7.75-10.90 80-420 7.25-8.45 245-552 2.63-41.32 <br />AR - 6 15 .4-17.3 7.27-11.30 84-215 7.40-8.70 248-555 2.63-41.32 <br />AR - 7 19 .2-17.4 7.35-11.30 81-412 7.45-8.80 276-555 2.63-41.32 <br />AR - 8 15 .2-17.4 7.38-11.40 89-214 7.40-8.70 262-565 2.63-41.32 <br />AR - 9 19 .2-17.1 7.25-11.40 74-412 7.45-8.55 270-560 4.81-58.86 <br /> <br />Current <br /> <br />Currents. usually related to flows (table 11. in- <br />creased during the spring runoff. The range of <br />flows during the study (fig. 7) increased signifi- <br />cantly from the upstream to the downstream <br />stations due to various inflows. <br /> <br />Substrate <br /> <br />The substrate sampled was similar throughout <br />the study area. except at AR-8. where it was <br />composed of larger material. <br /> <br />Water Chemistry <br /> <br />A summary of the major ions is given in table 2. <br />Specific physical and chemical parameters for <br />each sampling date are presented in tables A-1 <br />through A-20 of the appendix. Major ion con- <br />centrations at all river stations were within <br />acceptable ranges for the survival of aquatic or- <br />ganisms. The mean concentration of total <br />dissolved solids (TOSI increased downstream of <br />the Leadville Drain and California Gulch. but <br />decreased substantially downstream of the Lake <br />Fork inflow. Nitrogen and phosphorus com- <br />pounds (tables 2 and 31 enter the river in a <br />relatively high concentrations by way of Califor- <br />nia Gulch. <br /> <br />Heavy Metals <br /> <br />Means and standard deviations of selected <br />heavy metals are presented in figures 8 through <br />1 3. Mean concentrations of heavy metals during <br />high and low flows are shown in figures 14 <br />through 19. Specific concentrations throughout <br />the study period are presented in tables A-1 <br />through A-20 of the appendix. <br /> <br />Mean cadmium concentrations were in excess <br />of recommended levels at all stations except <br />EF-1. Copper enters the river in high concentra- <br />tions by way of California Gulch. Mean iron con- <br />centrations in the river were near recommended <br />levels upstream of California Gulch. but above <br />these levels after this metal-laden inflow enters <br />the river. Iron concentrations were highly related <br />to flows. and mean levels increased dramatically <br />downstream during increased runoff. This was <br />due to suspension of sediments and scouring of <br />the substrate. Lead concentrations were usually <br />above recommended limits. but below docu- <br />mented acute toxicity levels. Manganese con- <br />centrations were usually below recommended <br />limits for the protection of aquatic life at all sta- <br />tions except AR-3. High concentrations of man- <br />ganese entered the river from California Gulch. <br />Molybdenum was not detected in any river <br />samples and therefore would not likely pose a <br />toxicity problem. Mean zinc concentrations <br />exceeded recommended levels at all stations <br />except EF-1. The levels of zinc detected at AR-3 <br />indicated that it did not settle out rapidly and it <br />may be in a soluble and highly toxic form. <br /> <br />21 <br />